Home Multi-Country Search About Admin Login
Cenozoic
Mesozoic
Paleozoic
Neoproterozoic
Mesoproterozoic
Paleoproterozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Tuna Formation
Click to display on map of the Ancient World at:
Tuna Fm base reconstruction

Tuna Fm


Period: 
Paleogene

Age Interval: 
Rupelian (Early Oligocene)


Province: 
W.India Kutch Basin, W.India Saurashtra Basin

Type Locality and Naming

SUBSURFACE. Its type section is in Well GK-1-1, interval of 1225 to 1285 m. [Original Publication: Zutshi, P.L., Mittal, S.K and Shah, L. (1993) Lithostratigraphy of Indian Petroliferous Basins, Document IV, Kutch Saurashtra Basin, KDMIPE, ONGC Publication, pp 1-50.]. Reference well: Well OS-2-G-1, interval of 1360 to 1483 m.

[Fig. Geological and structural map of Kutch, also showing the onshore and offshore wells drilled for oil exploration. (Map by Rasoul Sorkhabi in GeoExpro Dec2014, based on various sources including S.K. Biswas, Current Science, 25May2005)]


Lithology and Thickness

Clayey limestone. Consists of limestone with minor shale and siltstone. 60m in GK-1-1, the thickness in Kutch offshore ranges from 15-115m. Towards Saurashtra its thickness increases further. In the well OS-2-G-1 in Saurashtra Basin, this formation consists of limestone with clays and carbonaceous matter. Towards Diu Arch, limestone facies of this formation changes into dominantly shaly facies.


Lithology Pattern: 
Clayey limestone


Relationships and Distribution

Lower contact

Unconformable with Fulra Limestone Fm. This boundary typically is marked by gamma and resistivity breaks on logs. This boundary also marked by last occurrences of Pellatispira zone in the Kutch shelf wells and Nummulites discorbis- Discocylina assemblages top in wells GKH-1 and Sutri-1 and top of Turborotalia cerruzoulesis top in other wells of Kutch.

Upper contact

Unconformable with the Narayan Sarovar Fm. It can be marked on the logs by increase in gamma and reduction in resistivity in the well KD-1.

[Figure 1: Biostratigraphic correlation in the Paleogene succession of Kutch offshore basin along section line A-B (after Anil Bhandari et al., 1996)]

Regional extent

Kutch and Saurashtra basin subsurface


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[67.55,22.63],[67.97,23.37],[68.51,23.97],[68.92,23.99],[68.94,24.29],[69.69,24.28],[69.87,24.17],[70.13,24.18],[70.2,24.28],[70.61,24.39],[70.59,24.24],[70.89,24.24],[70.99,24.33],[71.13,24.42],[71.02,24.45],[71,24.55],[71.1,24.65],[71.31,24.62],[71.39,24.37],[71.3,24.27],[71.33,23.97],[71.27,23.81],[71.63,23.35],[71.55,23.24],[71.34,23.27],[69.59,22.72],[68.13,22.15],[67.55,22.63]]]]}}

Fossils

Nummulites fichteli, Globerina tapuriensis


Age 

Rupelian (Early Oligocene)

Age Span: 

    Beginning stage: 
Rupelian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
33.90

    Ending stage: 
Rupelian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
27.29

Depositional setting

Varies from littoral to inner shelf to outer shelf.


Depositional pattern:  


Additional Information


Compiler:  

D.S.N Raju